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  • Postglacial sea-level rise in South Portugal as recorded in Guadiana Estuary
    Publication . Boski, T.; Moura, Delminda; Camacho, Sarita; Duarte, Duarte; Scott, David; Veiga-Pires, C.; Pedro, Paulo; Santana, Paulo
    The Guadiana River Estuary is located in the terminal part of a deeply incised river valley, which accumulated several tens of meters of sediments during the Holocenic transgression. Five cored boreholes (see Fig.1 for localisation) that reached the pre-Holocenic substratum were drilled recently in order to recognize the architecture of sedimentary facies and to quantify the accumulation of organic carbon trapped in sediments during the valley infilling by marine waters. It was assumed that due to structural constraints imposed by Palaeozoic and Mezozoic substratum, the main estuarine channel did not change its position significantly. Consequently borehole locations were chosen in order to represent different sedimentary environments in the estuary: proximity to the main channel (CM1 and CM3), external sea facing (CM4) and lagoonal (CM2 and CM5) environments.
  • Portuguese science needs a shakeup
    Publication . Boski, T.; Galvão, Helena M.
  • Ludo Formation-a new lithostratigraphic unit in Quaternary of Central Algarve
    Publication . Moura, Delminda; Boski, T.
    A new lithostratigraphic unit (Ludo Formation) is proposed aiming a more objective approach to mapping the Quaternary sedimentary series in the central Algarve.